LA's Island Playground Could Trigger Tsunamis

PASADENA, Calif. — Landslides coming off Catalina Island's steep slopes could send tsunamis racing toward popular Los Angeles and Orange County beaches with just a few minutes of warning, geoscientists said on April 23 here at the annual meeting of the Seismological Society of America.

The landslides were buried underwater because Catalina Island is sinking, said lead study author Chris Castillo, a Stanford University graduate student. The remnants of old beaches have dropped beneath the waves as the island descends, creating a stair-stepped series of nine terraces.

"Catalina is rare," Castillo told Live Science. "We knew there was evidence of subsidence, but it's the only [Southern California] island that has these submerged beaches."

Castillo does not yet know how fast Catalina Island is sinking. The oldest terrace is about 720 feet (220 m) below current sea level. The island is also tilting as it descends, which increases the landslide threat by destabilizing the steep coastal slopes, he added.

However, Castillo will soon get a better handle on the rate of sinking by matching the beach levels to well-known sea level changes during the past 1 million years. The research team plans to recover fossils from the terraces this summer, which will help connect Catalina's terraces to these past sea level events, he said. Currently, the researchers think the island is sagging by about 1 foot (30 centimeters) every 1,000 years.

Underwater terraces are evidence that Catalina Island is sinking and tilting.

Credit: Christ Castillo, Stanford University

Disaster planners have already recognized that California faces a rare but plausible tsunami risk from its iconic coastline. Major offshore fault lines have triggered small tidal waves during historic earthquakes. However, when these faults slip, the seafloor typically moves horizontally, without launching huge waves.

Instead, California's biggest local risk of deadly tsunamis comes from unpredictable underwater landslides. These avalanches shove seawater aside, setting off tsunamis. And in the new study, geologists found evidence of such enormous submarine landslides offshore Catalina Island.

Although tidal waves from submarine landslides only threaten local coastlines, the waves can kill. A submarine landslide triggered tsunamis that killed 2,200 people in Papua New Guinea in 1998.

"Landslides can have a big impact in a small area, and you don't get a lot of warning," said geophysicist Stephanie Ross, project leader for tsunami hazard scenarios for the U.S. Geological Survey in Menlo Park, California. Ross was not involved in the study.

But new geologic surveys are finding evidence that could heighten the tsunami risk. For instance, two earthquake faults offshore Ventura, between Santa Barbara and Los Angeles, shove the seafloor upward during quakes, according to research presented here Wednesday (April 22). This style of movement can generate tsunamis.

The two faults — the Pitas Point fault and the Red Mountain fault — could potentially unleash a magnitude-7 earthquake, said Kenny Ryan, a University of California, Riverside, graduate student. For the study, Ryan modeled tsunamis created by faults. He found that the waves turn counterclockwise toward the towns of Ventura and Oxnard once they hit deep water. "Tsunamis travel at different speeds depending on water depth," Ryan said.

Scientists are unsure how often tsunamis of any kind hit Southern California's coastline because there are few sand deposits onshore left by waves. The biggest study of tsunami deposits to date, published in 2014, looked for prehistoric tsunamis in 20 coastal locations and struck out at all but two.

So far, although the state has considered the new studies, its tsunami maps haven't needed revising, Wilson told Live Science. "These are very low-probability events," Wilson said.

Becky Oskin covers Earth science, climate change and space, as well as general science topics. Becky was a science reporter at Live Science and The Pasadena Star-News; she has freelanced for New Scientist and the American Institute of Physics. She earned a master's degree in geology from Caltech, a bachelor's degree from Washington State University, and a graduate certificate in science writing from the University of California, Santa Cruz.